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<br />2 <br /> <br />3 <br /> <br />4 <br /> <br />~ <br /> <br />I <br />I <br />l- <br />I <br />1- <br />:l <br />1- <br />:l <br />l- <br />I- <br />l <br />I~ <br />I.-~ <br />I- <br />I- <br />I- <br />I. <br />I <br />1 <br /> <br /> 100 - 81 <br />g [J:] <br />- <br />.. t:J. <br />J! <br />'& <br />'~ t:J. <br />Q. <br />- <br />0 ~ <br />.. <br />::t <br />.. <br />2 10 <br />0 <br />.. C <br />CJ' <br />.5 <br />"a 0 <br />. <br />. 8 cP c5> 0 <br />tit <br />0 0 <br />u t:J. C <br />;: 0 <br />.- <br />- <br />... <br />0 <br />.&: 1.0 -c;rA 0 <br />.... <br />.j 0 <br />.. <br />- <br />0 ~ <br />... 610 <br />c: 0 c9 <br />.2 0 0 0 0 <br />- <br />0 0 <br />.... <br />.a <br />.u 0 <br />.. C <br />.. <br />Q. <br />- 0.1 <br />0 <br />0 C <br />- 0 <br />0 <br />lr <br /> 0 <br /> <br />Altjtude ab9~' MSL pt <br />which precIpitation onQinate. <br /> <br /> <br />A. I. 5 km <br />C · 2.0 km <br />o · 2.5 km <br /> <br />CD <br /> <br />,01 <br /> <br />Ratio of horizontal displacement of precipitation from <br />point of oriQin to Qround ( artificially seeded I natural case) <br /> <br />Fig. 3,9 <br /> <br />Model predictions of the effects of ice particle concentration <br />on precipitation rate and horizontal path length of precipitation <br />for southwesterly flow (simulated blocking) over Cascade Mountains, <br />"Artificial seeding" refers to a concentration of ice particles of <br />25 or lOO.J -1 and "natural" refers to a concentration of l.R,-l, <br />